Orbital stability

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In mathematical physics and the theory of partial differential equations, the solitary wave solution of the form u(x,t)=e−iωtϕ(x) is said to be orbitally stable if any solution with the initial data sufficiently close to ϕ(x) forever remains in a given small neighborhood of the trajectory of e−iωtϕ(x).

Formal definition

Formal definition is as follows.[1] Consider the dynamical system

idudt=A(u),u(t)∈X,t∈ℝ,

with X a Banach space over ℂ, and A:X→X. We assume that the system is U(1)-invariant, so that A(eisu)=eisA(u) for any u∈X and any s∈ℝ.

Assume that ωϕ=A(ϕ), so that u(t)=e−iωtϕ is a solution to the dynamical system. We call such solution a solitary wave.

We say that the solitary wave e−iωtϕ is orbitally stable if for any ϵ>0 there is δ>0 such that for any v0∈X with ‖ϕ−v0‖X<δ there is a solution v(t) defined for all t≥0 such that v(0)=v0, and such that this solution satisfies

supt≥0infs∈ℝ‖v(t)−eisϕ‖X<ϵ.

Example

According to [2] ,[3] the solitary wave solution e−iωtϕω(x) to the nonlinear Schrödinger equation

i∂∂tu=−∂2∂x2u+g(|u|2)u,u(x,t)∈ℂ,x∈ℝ,t∈ℝ,

where g is a smooth real-valued function, is orbitally stable if the Vakhitov–Kolokolov stability criterion is satisfied:

ddωQ(ϕω)<0,

where

Q(u)=12∫ℝ|u(x,t)|2dx

is the charge of the solution u(x,t), which is conserved in time (at least if the solution u(x,t) is sufficiently smooth).

It was also shown,[4][5] that if ddωQ(ω)<0 at a particular value of ω, then the solitary wave e−iωtϕω(x) is Lyapunov stable, with the Lyapunov function given by L(u)=E(u)−ωQ(u)+Γ(Q(u)−Q(ϕω))2, where E(u)=12∫ℝ(|∂u∂x|2+G(|u|2))dx is the energy of a solution u(x,t), with G(y)=∫0yg(z)dz the antiderivative of g, as long as the constant Γ>0 is chosen sufficiently large.

See also

References